1.
Discussion on the Environmental Factors of Geologic Hazards Caused by a Creep Landslip in Youxi County
尤溪县蠕动滑坡地质灾害环境因素探讨
2.
Unsaturated Creep Model of the Sliding Zone Soils of Qianjiangping Landslide in Three Gorges
三峡千将坪滑坡滑动带土的非饱和蠕变模型
3.
According to this theory, ones can set up an empirical equation between deformation and time for predicting the time of failure of a landslide.
根据这一理论,人们可以建立早期滑动的唯象蠕变方程来预测滑坡。
4.
The slow movement of rock debris and soil down a weathered slope.
蠕动岩石碎片和土壤沿着受风雨侵蚀的滑坡向下缓慢移动
5.
PROCESSING AND PREDICTION OF THE DISPLACEMENT DATA FOR ROCK MASS CREEP--ATTRACTOR ANALYSIS OF SLOPE CREEP
岩体蠕变位移数据的处理和预测——滑坡蠕变吸引子分析
6.
The Research On Stability of Jinlongshan Landslide After the Reservoir Storing Water;
水库蓄水后金龙山谷坡Ⅱ区蠕滑体稳定性研究
7.
Numerical Simulation of Creep Behavior of Xiakou Landslide Under Different Rainfall Conditions
峡口滑坡不同降雨条件下蠕变行为分析
8.
Study on Creep Caused Landslide and Its Control in the Reservoir Area of the Three Gorges Based on the Modern Non-linear Sciences Gorges;
三峡库区边坡岩土体蠕滑与控制的现代非线性科学研究
9.
A controlled slide, in either a standing or sitting position, used in descending a steep icy or snowy incline.
滑降在下冰坡或雪坡时，或站或坐式的制动滑行
10.
Analysis of mechanical parameters of slip surface for basalt landslide in Yunnan
云南玄武岩滑坡滑动面力学参数分析
11.
Searching for Slip Surface and Stability Analysis of Colluvial Slope
堆积层滑坡滑动面搜寻及稳定性评价
12.
Grain boundary sliding in compressed olivine aggregates.
橄榄石集合体中与位错蠕变相伴随的粒间滑动
13.
Microscopic Marks of Stick Slip and Creep Slippage in Deformation Products along the Daqingshan Piedmont Active Fault
大青山山前活动断裂变形产物中的微观粘滑与蠕滑标志
14.
Dry Sliding Wear Research of Compacted Graphite Iron with Biomimetic Coupling Non-smooth Surfaces Processed by Laser;
仿生耦合非光滑表面蠕墨铸铁干滑动磨损性能研究
15.
STRENGTH OF DISTURBED CLAY IN SLIDING ZONE OF CIGU LANDSLIDE AND ASSOCIATED STABILITY ANALYSIS
茨菇滑坡滑带土扰动样强度参数取值分析及滑坡稳定性评价
16.
And the characteristics of homogeneous loess landslide and loess-mudstone cutting layer landslide are high sliding velocity, long sliding distance and high stability after sliding except its scarp.
黄土层内滑坡、土泥岩切层滑坡的滑速高、滑距长,滑体稳定性高。但后壁不稳定,易再次滑动。
17.
mass peristalsis
总体蠕动, 集团蠕动
18.
By the model, the whole sliding course can be simulated, and the maximum sliding speed and maximum sliding distance can be predicted.
应用该模型可以模拟滑坡发生后滑体运动的全过程,同时可预测滑坡的最大滑速和最大滑距。